Details
| Original language | English |
|---|---|
| Pages (from-to) | 194-200 |
| Number of pages | 7 |
| Journal | Applied Geochemistry |
| Volume | 85 |
| Publication status | Published - 29 May 2017 |
Abstract
In the course of the Fukushima Daiichi nuclear accident (March 2011), large quantities of radionuclides, mainly of the volatile elements such as cesium and iodine were released to the environment. In small amounts non-volatile elements such as plutonium and uranium have also been released. For this study vegetation, litter and soil drill core samples were taken in 2013 and 2015 in the contaminated area in Fukushima prefecture. In 2015 the samples were taken as close to the sampling locations of the 2013 campaign as possible. To investigate the origin of plutonium and uranium the isotopic ratios 240Pu/239Pu and 236U/238U were measured using accelerator mass spectrometry. While the determined 240Pu/239Pu ratios indicate global fallout as the plutonium source for most samples, reactor plutonium of the reactors of Fukushima Daiichi is identified unambiguously in some vegetation and litter samples. This assumption is corroborated by the detection of 236U. None of the samples contained higher plutonium activity concentrations than in the rest of Japan, caused by global fallout. This holds even for the samples where the reactors were identified as the source from the isotope ratios. This and the strong localization, even for neighboring sampling sites, indicate that the overall small quantities of plutonium were most likely released in the form of particulate matter.
Keywords
- Accelerator mass spectrometry, Fukushima nuclear accident, Plutonium, Uranium-236
ASJC Scopus subject areas
- Environmental Science(all)
- Environmental Chemistry
- Environmental Science(all)
- Pollution
- Earth and Planetary Sciences(all)
- Geochemistry and Petrology
Cite this
- Standard
- Harvard
- Apa
- Vancouver
- BibTeX
- RIS
In: Applied Geochemistry, Vol. 85, 29.05.2017, p. 194-200.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Radionuclide pollution inside the Fukushima Daiichi exclusion zone, part 2
T2 - Forensic search for the “Forgotten” contaminants Uranium-236 and plutonium
AU - Schneider, Stephanie
AU - Bister, Stefan
AU - Christl, Marcus
AU - Hori, Mayumi
AU - Shozugawa, Katsumi
AU - Synal, Hans Arno
AU - Steinhauser, Georg
AU - Walther, Clemens
PY - 2017/5/29
Y1 - 2017/5/29
N2 - In the course of the Fukushima Daiichi nuclear accident (March 2011), large quantities of radionuclides, mainly of the volatile elements such as cesium and iodine were released to the environment. In small amounts non-volatile elements such as plutonium and uranium have also been released. For this study vegetation, litter and soil drill core samples were taken in 2013 and 2015 in the contaminated area in Fukushima prefecture. In 2015 the samples were taken as close to the sampling locations of the 2013 campaign as possible. To investigate the origin of plutonium and uranium the isotopic ratios 240Pu/239Pu and 236U/238U were measured using accelerator mass spectrometry. While the determined 240Pu/239Pu ratios indicate global fallout as the plutonium source for most samples, reactor plutonium of the reactors of Fukushima Daiichi is identified unambiguously in some vegetation and litter samples. This assumption is corroborated by the detection of 236U. None of the samples contained higher plutonium activity concentrations than in the rest of Japan, caused by global fallout. This holds even for the samples where the reactors were identified as the source from the isotope ratios. This and the strong localization, even for neighboring sampling sites, indicate that the overall small quantities of plutonium were most likely released in the form of particulate matter.
AB - In the course of the Fukushima Daiichi nuclear accident (March 2011), large quantities of radionuclides, mainly of the volatile elements such as cesium and iodine were released to the environment. In small amounts non-volatile elements such as plutonium and uranium have also been released. For this study vegetation, litter and soil drill core samples were taken in 2013 and 2015 in the contaminated area in Fukushima prefecture. In 2015 the samples were taken as close to the sampling locations of the 2013 campaign as possible. To investigate the origin of plutonium and uranium the isotopic ratios 240Pu/239Pu and 236U/238U were measured using accelerator mass spectrometry. While the determined 240Pu/239Pu ratios indicate global fallout as the plutonium source for most samples, reactor plutonium of the reactors of Fukushima Daiichi is identified unambiguously in some vegetation and litter samples. This assumption is corroborated by the detection of 236U. None of the samples contained higher plutonium activity concentrations than in the rest of Japan, caused by global fallout. This holds even for the samples where the reactors were identified as the source from the isotope ratios. This and the strong localization, even for neighboring sampling sites, indicate that the overall small quantities of plutonium were most likely released in the form of particulate matter.
KW - Accelerator mass spectrometry
KW - Fukushima nuclear accident
KW - Plutonium
KW - Uranium-236
UR - http://www.scopus.com/inward/record.url?scp=85021316433&partnerID=8YFLogxK
U2 - 10.1016/j.apgeochem.2017.05.022
DO - 10.1016/j.apgeochem.2017.05.022
M3 - Article
AN - SCOPUS:85021316433
VL - 85
SP - 194
EP - 200
JO - Applied Geochemistry
JF - Applied Geochemistry
SN - 0883-2927
ER -